Prof. Dr. Marta E. Torres
Projekte & Publikationen
When sites of methane discharge on the seafloor were discovered offshore Oregon and Washington (U.S) in 1985, it was clear that they represented a new and important research arena. We needed to understand the mechanisms that drive the methane discharge, the origins of the fluids that carry the methane and the consequences that this process has on the geology and biology of the margin. Since then, myself and other scientists have participated in many expeditions to this and similar margins, which have provided significant and incremental knowledge. Among these advances is our realization that some of the methane in the sediment is sequestered into solid structures called gas hydrates. Gas hydrates are stable only within a sediment sliver that terminates at about 500 meters of water depth and their stability may be impacted by changes in bottom water temperatures. A new, MARUM-led expedition to the Cascadia margin is planned for 2025. My time at HWK will be dedicated to integrating existing information gathered thus far in this region (and elsewhere) in conjunction with scientists from the University of Bremen and the Alfred Wegener Institute. Together, we will develop strategies for an integrated field program to tackle outstanding questions regarding fluid-rock-biology interactions, their response to changing oceanic conditions, and the potential role they may play in earthquake generation.